Global observations of stratospheric gravity. comparisons with an atmospheric general circulation model

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Global observations of stratospheric gravity waves made with COSMIC GPS RO and comparisons with an atmospheric general circulation model S. P. Alexander 1, T. Tsuda 2, Y. Kawatani 3, M.

1 Global observations of stratospheric gravity waves made with COSMIC GPS RO and comparisons with an atmospheric general circulation model S. P. Alexander 1, T. Tsuda 2, Y. Kawatani 3, M. Takahashi 4, K. Sato 5 and A. R. Klekociuk 1 1 Australian Antarctic Division, Hobart, Australia. 2 RISH, Kyoto University, Japan 3 FRCGC, JAMSTEC, Yokohama, Japan 4 CCSR, University of Tokyo, Kashiwa, Japan 5 Department of Earth and Planetary Sciences, University of Tokyo, Tokyo, Japan

2 Outline GPS RO background: GPS/MET and CHAMP COSMIC and T106L60 model comparisons Tropical gravity waves Equatorially trapped waves Extra tropical gravity waves Gravity waves in the polar regions Orographic gravity waves and Polar Stratospheric Clouds (PSCs)

GPS RO: Setting the scene (1/2) GPS/MET in the mid 90s provided

CHAMP provided a multi year dataset for wave analyses GPS Radio

vertical group velocities and with short vertical wavelengths

3 GPS RO: Setting the scene (1/2) GPS/MET in the mid 90s provided the first global picture of gravity wave activity using GPS RO CHAMP provided a multi year dataset for wave analyses GPS Radio Occultations are more likely to capture gravity waves with slow vertical group velocities and with short vertical wavelengths (contrast with e.g. MLS) Tsuda et al., 2000 de la Torre et al., 2006

4 GPS RO: Setting the scene (2/2) Polar observations using CHAMP showed large orographic gravity wave activity above the Peninsula and Trans Antarctic Mountains as well as the relationship between large gravitywave activity and strong winds Baumgaertner & McDonald, 2007 Hei et al., 2008

Tropical gravity waves COSMIC results for September 2007 Winds were westward below 32km Large potential energy is visible directly above deep convective

5 Tropical gravity waves COSMIC results for September 2007 Winds were westward below 32km Large potential energy is visible directly above deep convective activity. Slow c x > 0 waves are encountering their critical level (group velocities also decrease close to critical levels, increasing the chance of wave observation.)

6 Model results of PE in westward QBO shear phase shown (model incorporates wider range of GWs than COSMIC) Top panel shows distribution at 100hPa Bottom panel shows PE near the u = 0 m s 1 line: increased PE above deep convective regions Tropical gravity waves

Equatorially trapped waves Investigate with COSMIC data: slow Kelvin waves with 8 < h e < 90 m, corresponding to λ z less than ~8 km (h e = 90 m corresponds to c x = 30 ms 1 ) MRGWs with 8 <

7 Equatorially trapped waves Investigate with COSMIC data: slow Kelvin waves with 8 < h e < 90 m, corresponding to λ z less than ~8 km (h e = 90 m corresponds to c x = 30 ms 1 ) MRGWs with 8 < h e < 90 m. While we can theoretically observe n=1 ER and n=0 EIGW, the resultant wave structures appear noisy and / or show little height consistency (there isn t much power in these bands)

8 Equatorially trapped waves 22km slow Kelvin waves observed by COSMIC for January July 2007 OLR 220 W m 2 marked in white Kelvin waves are mostly k = 1, 2 with periods ~ days and c x ~ m s 1

Equatorially trapped waves 22km Mixed Rossby Gravity Waves observed by COSMIC for January July 2007 (these waves are visible in the unfiltered anti symmetric data although there may be some GW

9 Equatorially trapped waves 22km Mixed Rossby Gravity Waves observed by COSMIC for January July 2007 (these waves are visible in the unfiltered anti symmetric data although there may be some GW contamination) Wave packet behaviour evident: packets propagate eastward while the waves propagate westward Decrease in amplitudes after May: QBO is westward after this time thus removing MRGWs Periods 3 5 days, amplitudes up to ~1.2K, c x ~ m s 1, k > 5

QBO westward shear phase in the lower stratosphere The model s

10 Equatorially trapped waves Both model (LHS) and observations (RHS) show Kelvin waves propagating upward and eastward during QBO westward shear phase in the lower stratosphere The model s arrows are the energy flux, which are parallel to intrinsic group velocity

Extra tropical gravity waves COSMIC E p (LHS) for 12 18 Dec 2006 at 140E AGCM

vertical energy fluxes due to λ z < 7km Large PE along the equatorward side of

11 Extra tropical gravity waves COSMIC E p (LHS) for Dec 2006 at 140E AGCM E p (RHS) for 1 7 Jan (similar wind conditions): vectors show meridional and vertical energy fluxes due to λ z < 7km Large PE along the equatorward side of observed and modeled jet from mid troposphere up to polar night jet COSMIC AGCM

Extra tropical gravity waves COSMIC NH winter 2006 07 mean E p at 20km (colour); NCEP 500 100hPa u (red); precipitation

12 Extra tropical gravity waves COSMIC NH winter mean E p at 20km (colour); NCEP hPa u (red); precipitation (mm/day, black) Enhanced E p above the Canadian Rockies, Scandinavia (orographically related); Japan, eastern US (jet related)

13 Gravity waves in the polar regions COSMIC resolves more intermittent orographic waves than CHAMP due to the larger amount of occultation events Evidence of gravity wave Doppler shifting and orographicwave activity in monthly averages

Gravity waves in the polar regions The σ 2 relative to the vortex edge on isentropic surfaces Above 600K, the largest σ 2 correspond to the strongest winds at

14 Gravity waves in the polar regions The σ 2 relative to the vortex edge on isentropic surfaces Above 600K, the largest σ 2 correspond to the strongest winds at the vortex edge (Doppler shifting) Below 600K, larger σ 2 occur equatorward of the vortex edge, suggesting sub tropical or mid latitude wave sources. Pole Eq Pole

Gravity waves in the polar regions Time series of 2006 07 NH σ 2 in

during winter and the poleward movement of large σ 2 is seen,

upward and into the stratospheric jet Large increases in σ 2 inside the

15 Gravity waves in the polar regions Time series of NH σ 2 in equivalent latitudes at 450K: The poleward movement of the vortex edge during winter and the poleward movement of large σ 2 is seen, indicating poleward propagation of waves which are then likely focussed upward and into the stratospheric jet Large increases in σ 2 inside the vortex at the start of Jan and Feb at times of minor SSWs Vortex edge (thick yellow)

16 Gravity waves in the polar regions Large stratospheric σ 2 above mountain ranges are observed intermittently throughout winter, when there is relatively low wind rotation angle in the troposphere. Scandinavia (LHS) and the Antarctic Peninsula (RHS): σ 2 at 500K, 800K, 1000K Wind rotation angle (solid)

orographic gravity wave activity above the Antarctic Peninsula, are these

17 Orographic gravity wave activity and Polar Stratospheric Clouds (PSCs) Question: Given that with COSMIC we can observe relatively short (< 1 week) variations in orographic gravity wave activity above the Antarctic Peninsula, are these observable waves likely responsible for initiating the production of any PSCs? Answer: YES!

18 Orographic gravity wave activity and Polar Stratospheric Clouds (PSCs) Alexander, Klekociuk, Pitts, McDonald and Arevalo Torres, JGR (2011), in press Poster on Tuesday afternoon But, just to recap Obtain PSC composition classes from CALIPSO lidar data (H 2 O ice, STS, and two liquid / NAT mixed classes) during the 2007 austral winter. Then combine PSC results with COSMIC gravity wave σ 2 and MLS (for T T ice and T T NAT )

19 Orographic gravity wave activity and Polar Stratospheric Clouds (PSCs) Antarctic Peninsula at 60 70S: mid May to mid October 2007 COSMIC temperatures (colour contour)

20 Orographic gravity wave activity and Polar Stratospheric Clouds (PSCs) Antarctic Peninsula at 60 70S: mid May to mid October 2007 COSMIC temperatures (colour contour) COSMIC σ 2 (red lines, units of K 2 ) intermittent, large orographic waves

21 Orographic gravity wave activity and Polar Stratospheric Clouds (PSCs) Antarctic Peninsula at 60 70S: mid May to mid October 2007 COSMIC temperatures (colour contour) COSMIC σ 2 (red lines, units of K 2 ) intermittent, large orographic waves CALIPSO H 2 O ice area (thick: 0.02 million km 2, thin: 0.1 million km 2 )

22 Orographic gravity wave activity and Polar Stratospheric Clouds (PSCs) Large H 2 O ice volumes above Peninsula when have large orographic gravity wave σ 2 Increased NAT volumes for considerable distances downstream OGWs needed in addition to PWs to explain PSCs

23 Summary COSMIC observations and T106L60 model studies of equatorially trapped waves and convectively generated gravity waves in the tropics show good agreement. COSMIC observes gravity waves directly above convection, Kelvin waves and Mixed Rossby Gravity Waves. Gravity waves observed by COSMIC and generated in the midlatitudes are likely focussed into the winter stratospheric jets. Doppler shifting of waves by the background winds occurs. The regional variability of orographic and non orographic waves in the polar regions is seen with COSMIC, over subweekly time scales. Orographic gravity waves above the Antarctic Peninsula induce the formation of polar stratospheric clouds (water ice and then NAT downstream) in the lower stratosphere.

24 References Alexander, S. P., T. Tsuda and Y. Kawatani (2008), COSMIC GPS Observations of Northern Hemisphere Winter Stratospheric Gravity Waves and Comparisons with an Atmospheric General Circulation Model, Geophysical Research Letters, 35, L10808, doi: /2008gl Alexander, S. P., T. Tsuda, Y. Kawatani and M. Takahashi (2008), Global distribution of atmospheric waves in the equatorial upper troposphere and lower stratosphere: COSMIC observations of wave mean flow interactions, Journal of Geophysical Research, 113, D24115, doi: /2008jd Kawatani, Y., M. Takahashi, K. Sato, S. P. Alexander and T. Tsuda (2009), Global distribution of atmospheric waves in the equatorial upper troposphere and lower stratosphere: AGCM simulation of sources and propagation, Journal of Geophysical Research, 114, D01102, doi: /2008jd Alexander, S. P., A. R. Klekociuk and T. Tsuda (2009), Gravity wave and orographic wave activity observed around the Antarctic and Arctic stratospheric vortices by the COSMIC GPS RO satellite constellation, Journal of Geophysical Research, 114, D17103, doi: /2009jd Alexander, S. P., A. R. Klekociuk, M. C. Pitts, A. J. McDonald, and A. Arevalo Torres (2011), The effect of orographic gravity waves on Antarctic Polar Stratospheric Cloud (PSC) occurrence and composition, Journal of Geophysical Research, doi: /2010jd015184, in press

Global studies of stratospheric gravity wave. Simon Alexander 1, Toshitaka Tsuda 2, Andrew Klekociuk 1, Yoshio Kawatani 3, and Masaaki Takahasi 4

Global studies of stratospheric gravity wave activity using COSMIC GPS-RO Simon Alexander 1, Toshitaka Tsuda 2, Andrew Klekociuk 1, Yoshio Kawatani 3, and Masaaki Takahasi 4 1 Australian Antarctic Division,